Carboniferous deposits in the basement of the southwestern West Siberian geosyneclise (Kurgan Region)
статья в журнале
(ИНГГ СО РАН)
(ИНГГ СО РАН)
(ИГМ СО РАН)
дата публикации: 2016
The Ar-40/Ar-39 age of volcanics from the sections of core boreholes in the northern Tyumen'-Kostanai trough (Kurgan Region) has been determined. The geologic structure of the northern part of the trough has been refined. The paleogeographic environments and geodynamic settings of formation of Carboniferous deposits have been established by sedimentological, petrological, and geochemical studies of the sections. In the Visean, marine environments with maximum basin depths were predominant. In the Kachar epoch (C1v3-s), the submarine relief of the basin became more complicated; blocks of older rocks appeared in the deposits. The geochemical indicator characteristics of the volcanics-contents of HFSE (Ti, Nb, Ta, Th, and Hf)-are close to those of andesitoids of island arcs and Andean-type active continental margins, as well as present-day andesites from the Kurile-Kamchatka zone. They are an order of magnitude lower than those in similar continental-rift volcanics, among which are volcanics of the Valer'yanovka zone (according to some researchers). The contents of Ni, Co, and V are similar to those in island-arc andesites, including rocks of the Kurile-Kamchatka zone.
первоисточник: Russian Geology and Geophysics